FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1976450780> ?p ?o ?g. }

• W1976450780 endingPage "13" @default.
• W1976450780 startingPage "ACH 4" @default.
• W1976450780 abstract "[1] We assess the viability of diagnosing polar stratospheric cloud (PSC) composition and denitrification using existing satellite measurements. A Lagrangian approach is used to track PSC evolution from formation through dissipation. Upper Atmosphere Research Satellite Microwave Limb Sounder observations of gas-phase HNO3 and Polar Ozone and Aerosol Measurement II observations of aerosol extinction from the Arctic late winter of 1995/1996 are correlated and compared to results from PSC composition models along air parcel trajectories. This approach is successful in capturing the broad patterns of PSC development. That is, a strong correlation is found between low-temperature, low-HNO3, and high-extinction points. In most cases the observed behavior along the Lagrangian paths falls within the range predicted by equilibrium liquid ternary aerosol and nitric acid trihydrate composition models. At no time along the trajectories (when there is data coverage) do the models display large changes in either HNO3 or aerosol extinction that are not reflected in the data. In general, however, there is a large degree of overlap in the comparisons between the models and the data. Unmeasured quantities and large uncertainties in both measurements and model calculations preclude conclusive determination of PSC composition or phase in most cases. In the majority of PSC events studied, gas-phase HNO3 fully recovers to pre-PSC abundances following cloud evaporation. We conclude that while severe denitrification (50% or greater) may have occurred in highly localized regions in the Arctic in 1996, it did not occur over spatial scales comparable to or larger than the MLS field of view (∼400 km × 200 km × 6 km), even though it was a relatively cold winter. Improved measurements from upcoming satellite missions, such as Earth Observing System Aura, will ameliorate many of the difficulties in diagnosing PSC composition and denitrification encountered in this study." @default.
• W1976450780 created "2016-06-24" @default.
• W1976450780 creator A5028912961 @default.
• W1976450780 creator A5056049303 @default.
• W1976450780 creator A5056460069 @default.
• W1976450780 creator A5059739214 @default.
• W1976450780 creator A5065613655 @default.
• W1976450780 creator A5073274045 @default.
• W1976450780 creator A5083553398 @default.
• W1976450780 date "2002-05-27" @default.
• W1976450780 modified "2023-09-30" @default.
• W1976450780 title "A Lagrangian approach to studying Arctic polar stratospheric clouds using UARS MLS HNO3and POAM II aerosol extinction measurements" @default.
• W1976450780 cites W1499913620 @default.
• W1976450780 cites W164597573 @default.
• W1976450780 cites W1963694552 @default.
• W1976450780 cites W1967349557 @default.
• W1976450780 cites W1969762840 @default.
• W1976450780 cites W1969859259 @default.
• W1976450780 cites W1977072837 @default.
• W1976450780 cites W1977343561 @default.
• W1976450780 cites W1979925313 @default.
• W1976450780 cites W1980667530 @default.
• W1976450780 cites W1982325373 @default.
• W1976450780 cites W1983377326 @default.
• W1976450780 cites W1986862501 @default.
• W1976450780 cites W1987831533 @default.
• W1976450780 cites W1988069708 @default.
• W1976450780 cites W1990503413 @default.
• W1976450780 cites W1990942539 @default.
• W1976450780 cites W1993202987 @default.
• W1976450780 cites W1994653329 @default.
• W1976450780 cites W1995179926 @default.
• W1976450780 cites W1996380933 @default.
• W1976450780 cites W1997973977 @default.
• W1976450780 cites W1998322515 @default.
• W1976450780 cites W1998620652 @default.
• W1976450780 cites W1998830750 @default.
• W1976450780 cites W2001584906 @default.
• W1976450780 cites W2002356052 @default.
• W1976450780 cites W2004023705 @default.
• W1976450780 cites W2010129454 @default.
• W1976450780 cites W2010598341 @default.
• W1976450780 cites W2012792564 @default.
• W1976450780 cites W2021900241 @default.
• W1976450780 cites W2022755951 @default.
• W1976450780 cites W2022922452 @default.
• W1976450780 cites W2026673973 @default.
• W1976450780 cites W2029671768 @default.
• W1976450780 cites W2030329289 @default.
• W1976450780 cites W2035583260 @default.
• W1976450780 cites W2036683456 @default.
• W1976450780 cites W2038106926 @default.
• W1976450780 cites W2039025224 @default.
• W1976450780 cites W2042678889 @default.
• W1976450780 cites W2050334623 @default.
• W1976450780 cites W2058556608 @default.
• W1976450780 cites W2058631050 @default.
• W1976450780 cites W2067425152 @default.
• W1976450780 cites W2071618756 @default.
• W1976450780 cites W2073342050 @default.
• W1976450780 cites W2073887984 @default.
• W1976450780 cites W2075501990 @default.
• W1976450780 cites W2081097978 @default.
• W1976450780 cites W2081766633 @default.
• W1976450780 cites W2083410171 @default.
• W1976450780 cites W2088545517 @default.
• W1976450780 cites W2089987564 @default.
• W1976450780 cites W2092168539 @default.
• W1976450780 cites W2092502604 @default.
• W1976450780 cites W2093035552 @default.
• W1976450780 cites W2095176597 @default.
• W1976450780 cites W2112253639 @default.
• W1976450780 cites W2124594100 @default.
• W1976450780 cites W2125698412 @default.
• W1976450780 cites W2127024102 @default.
• W1976450780 cites W2135215024 @default.
• W1976450780 cites W2141929447 @default.
• W1976450780 cites W2172238670 @default.
• W1976450780 cites W2172801746 @default.
• W1976450780 cites W2173251738 @default.
• W1976450780 cites W36500372 @default.
• W1976450780 doi "https://doi.org/10.1029/2000jd000227" @default.
• W1976450780 hasPublicationYear "2002" @default.
• W1976450780 type Work @default.
• W1976450780 sameAs 1976450780 @default.
• W1976450780 citedByCount "15" @default.
• W1976450780 countsByYear W19764507802014 @default.
• W1976450780 countsByYear W19764507802015 @default.
• W1976450780 countsByYear W19764507802018 @default.
• W1976450780 crossrefType "journal-article" @default.
• W1976450780 hasAuthorship W1976450780A5028912961 @default.
• W1976450780 hasAuthorship W1976450780A5056049303 @default.
• W1976450780 hasAuthorship W1976450780A5056460069 @default.
• W1976450780 hasAuthorship W1976450780A5059739214 @default.
• W1976450780 hasAuthorship W1976450780A5065613655 @default.
• W1976450780 hasAuthorship W1976450780A5073274045 @default.
• W1976450780 hasAuthorship W1976450780A5083553398 @default.
• W1976450780 hasBestOaLocation W19764507801 @default.

• next